Temporal changes in SOM, N, P, K, and their stoichiometric ratios during reforestation in China and interactions with soil depths: Importance of deep-layer soil and management implications
• Larch afforestation induced SOM accumulation in surface but depletion in deep soil. • Total N, P, their extractable forms peaked at 20–40-yr, but depleted in >40-yr forest. • Nearly 50% of SOM and N was in 0–20cm soil, but >60% of P and K was in deep soils. • >30% Increases in C:N, C:P, K...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Wang, Wenjie [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2014 |
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| Schlagwörter: |
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| Umfang: |
10 |
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| Übergeordnetes Werk: |
Enthalten in: A new phenomenological constitutive model for hot tensile deformation behaviors of a typical Al–Cu–Mg alloy - Lin, Y.C. ELSEVIER, 2013, Amsterdam [u.a.] |
|---|---|
| Übergeordnetes Werk: |
volume:325 ; year:2014 ; day:1 ; month:08 ; pages:8-17 ; extent:10 |
| Links: |
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| DOI / URN: |
10.1016/j.foreco.2014.03.023 |
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Temporal changes in SOM, N, P, K, and their stoichiometric ratios during reforestation in China and interactions with soil depths: Importance of deep-layer soil and management implications |
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• Larch afforestation induced SOM accumulation in surface but depletion in deep soil. • Total N, P, their extractable forms peaked at 20–40-yr, but depleted in >40-yr forest. • Nearly 50% of SOM and N was in 0–20cm soil, but >60% of P and K was in deep soils. • >30% Increases in C:N, C:P, K:P and K:extractable K were observed in >40-yr forest. |
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• Larch afforestation induced SOM accumulation in surface but depletion in deep soil. • Total N, P, their extractable forms peaked at 20–40-yr, but depleted in >40-yr forest. • Nearly 50% of SOM and N was in 0–20cm soil, but >60% of P and K was in deep soils. • >30% Increases in C:N, C:P, K:P and K:extractable K were observed in >40-yr forest. |
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• Larch afforestation induced SOM accumulation in surface but depletion in deep soil. • Total N, P, their extractable forms peaked at 20–40-yr, but depleted in >40-yr forest. • Nearly 50% of SOM and N was in 0–20cm soil, but >60% of P and K was in deep soils. • >30% Increases in C:N, C:P, K:P and K:extractable K were observed in >40-yr forest. |
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Temporal changes in SOM, N, P, K, and their stoichiometric ratios during reforestation in China and interactions with soil depths: Importance of deep-layer soil and management implications |
| url |
https://doi.org/10.1016/j.foreco.2014.03.023 |
| remote_bool |
true |
| author2 |
Wang, Huimei Zu, Yuangang |
| author2Str |
Wang, Huimei Zu, Yuangang |
| ppnlink |
ELV011513292 |
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z |
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false |
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| author2_role |
oth oth |
| doi_str |
10.1016/j.foreco.2014.03.023 |
| up_date |
2024-07-06T17:05:10.921Z |
| _version_ |
1803850099902644224 |
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